From 125b0c6d67d857b9a2e07d6e301ae6a08716f992 Mon Sep 17 00:00:00 2001 From: Hal Simpson <hasimpson@usgs.gov> Date: Tue, 17 Feb 2015 21:32:17 -0700 Subject: [PATCH] another test on tables --- docs/XYZ.md | 19 ++++++++++++------- 1 file changed, 12 insertions(+), 7 deletions(-) diff --git a/docs/XYZ.md b/docs/XYZ.md index fa7e53d21..89a447fc2 100644 --- a/docs/XYZ.md +++ b/docs/XYZ.md @@ -13,9 +13,14 @@ Historically, the most common coordinate system used to specify measured geomagn -1. H is the magnitude of the geomagnetic field vector tangential to the Earth’s surface; -2. D is the declination, or clockwise angle from the vector pointing to the geographic north pole to the H vector; -3. Z is the downward component of the geomagnetic field. +<dl> + <dt>H</dt> + <dd>is the magnitude of the geomagnetic field vector tangential to the Earth’s surface;</dd> + <dt>D</dt> + <dd> is the declination, or clockwise angle from the vector pointing to the geographic north pole to the H vector;</dd> + <dt>Z</dt> + <dd>is the downward component of the geomagnetic field.</dd> +</dl> @@ -73,11 +78,11 @@ One thing that is not labeled in this figure is the angle d (see Eq. 4), which i Equations 4, 5, and 6 describe how to convert the horizontal components of a USGS magnetometer’s raw data element into more standard H and D components. -#|Equation + 1 |Equation ---|----------------------- -|(4) -|(5) -|(6) +|(4)| +|(5)| +|(6)| -- GitLab